Riset Geologi dan Pertambangan Volume 34 No 1 (2024)

Dear RGP readers,


We present the first issue of Volume 34 of Riset Geologi dan Pertambangan (Geology and Mining Research). This issue publishes five articles that covered topics on hydrogeology, mining, petrology, and geochemistry. In the first article, Mareta et al. present the water critically index of Welaran area in Central Java, Indonesia. The higher the WCI value, the more concerned the water conditions in the area will be. The water crisis can be handled if various parties manage water resources following good management. The Welaran area is part of the Lukulo Watershed, where the population often experiences water shortages. In 2020, Karangsambung has been designated as a part of Kebumen Global Geopark, which will certainly increase the number of tourists visiting here. The increase in tourist visits will also increase the need for water, including in the Welaran Watershed. The second article by Kasih et al. briefly explained mine drainage system design in a coal mine in Kalimantan, Indonesia. This mine drainage system aims to ensure that mining activity areas are not flooded during the rainy season. The drainage system consists of designing sump dimensions, open
channels, settling ponds, and pumping and piping systems. In the third paper, Al Kausar et al. elucidate geochemical analysis, including major, trace and rare earth
elements, conducted by fusion ICP-MS to find out the different composition of volcanic rocks in the Karaha-Talagabodas fields in West Java, Indonesia. The major element diagram shows the sampled rocks consist of calc-alkaline for andesite of Karaha and basalt, basaltic andesite, and andesite of tholeiitic environments for the Talagabodas volcanic rocks. The normalized REE diagram of N-MORB shows the similarity of the pattern of all Talagabodas volcanic rocks, whereas the Karaha andesite rocks show
slight REE enrichment and europium depletion. The next article investigates the possibility of using flotation process wastes from Buzlukdağı feldspar beneficiation plant, Türkiye as an alternative raw material. Ozgul & Ozcelik evaluate the use of wastes from feldspar enrichment and feldspar processes as alternative raw materials in another process and investigating their usability as a final product in various sectors and fields. The results show that the process can be used for technological purposes. Furthermore, the wastes from the enrichment can be used to provide permeability in urban waste storage areas and hydroelectric dam construction.
In the last paper, based on analyses of published geological data, Abdalla et al. reviewed several possible mechanisms of this backarc thrust in western Java. Previous works proposed that the backarc thrust in western Java may have developed as deformation of paleo-accretionary wedge sediments behind a continental backstop, inverted normal fault, northward migrating thrust belt, and thrusting due to
gravitational sliding of the volcanic arc. However, evidences supporting those mechanisms still need to be elucidated.


Riset Geologi dan Pertambangan – Geology and Mining Research welcomes your contributions in the forthcoming issues. We sincerely acknowledge all the authors and outstanding reviewers for their valuable contributions to this issue. We recognize all the editorial members and staffs for their continuous fineness support for the publication of this volume.
The Editors

Detil struktur seismik di bawah zona gempa Yogyakarta 2006 (Mw ∼6.4), Indonesia berdasarkan tomografi gempa lokal (Librian et al., PEPI, 2024)

Paper yang ditulis oleh Mas Virga (BMKG) beserta kawan-kawan dari ITB, BRIN, GFZ, dan UGM ini mengulas mengenai detil struktur kegempaan yang terjadi 18 tahun yang lalu di Yogyakarta. Gempa bumi yang terjadi pada tanggal 26 Mei 2006 dengan magnitud Mw ∼6,4 ini merupakan salah satu gempa bumi paling merusak di Indonesia. Gempa tersebut menimbulkan ribuan korban jiwa, puluhan ribu luka-luka, dan ratusan ribu kerusakan rumah di wilayah Yogyakarta dan sekitarnya dengan kerugian yang besar. Studi sebelumnya dari tomografi seismik dan pencitraan radar satelit berhipotesis bahwa gempa tersebut disebabkan oleh aktifnya sesar yang sejauh ini tidak diketahui di sebelah timur Sesar Opak. Padahal, sesar Opak awalnya diduga menjadi sumber terjadinya gempa tersebut. Dugaan tersebut muncul karena kerusakan terparah terjadi di wilayah Bantul sebelah barat Sesar Opak. Studi ini menunjukkan bahwa tomografi seismik kami mempunyai resolusi yang lebih tinggi dibandingkan penelitian sebelumnya dan dapat menggambarkan sistem sesar yang terjadi. Kami memanfaatkan lebih banyak gempa susulan dan ukuran grid yang lebih kecil untuk inversi tomografi seismik. Kami berhasil menggambarkan Sesar Opak dan sesar kedua yaitu Sesar Ngalang pada kedalaman 9 km. Dua sesar ini ditunjukkan oleh kontras kecepatan Vp, rasio Vp/Vs, dan Vs dari tomogram bagian horizontal. Kedua sesar tersebut dihubungkan oleh Sesar Oyo yang patahnya berlawanan arah dibandingkan kedua sesar tersebut. Semoga bermanfaat. Salam.

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